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generation peak
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  生油高峰
     The oil mature parameter indicates that the oil is at the generation peak and equal to a stage of R_o from 0.8% to 1.0%.
     成熟度参数表明原油成熟度相当于Ro值为0.8%~1.0%阶段,是生油高峰阶段。
短句来源
     4.Presenting the model of hydrocarbon formation-expulsion of source rock, and pointing out that threshold of oil generation in Wuerxun Sag's is 1550m, the generation peak is 2200m, the expulsion threshold is 1700m.
     4、建立了源岩的生排烃模式,指出乌尔逊凹陷生油门限为1550m,生油高峰为2200m,排油门限为1700m。
短句来源
     Oil generated of interval ES3 source rock is also centrally in Haitongji Sag. It reachedhydrocarbon threshold when it is buried 2800m deep with Ro 0.5% while it reachedoil generation peak when it is buried 4000m deep with Ro 1.3%.
     沙三段烃源岩生油中心也位于海通集洼陷,埋深达到 2800m 时,Ro 为 0.5%,达到生烃门限; 埋深 4000m 时,Ro 为 1.3%,达到生油高峰
短句来源
     the Ro was over 3. 0% in deep Baiyun Sag. The hydrocarbon generation had started at about 27Ma ago and oil generation peak occurred at about 22Ma ago,and its hydrocarbon generation time was obviously earlier than that at the slope belt of the sag margin.
     白云凹陷深凹处镜质体反射率大于3.0%,大约在距今27Ma开始生烃,在距今大约22Ma达到生油高峰,生烃时间明显早于凹陷边缘斜坡带。
短句来源
     After oil generation peak,the amount of gaseous hydrocarbons begins increasing rapidly because of splitting of liquid products.
     生油高峰之后由于液态产物的大量热裂解才开始进入气态烃的大量生成阶段。
短句来源
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  烃高峰
     fusinite has two hydrocarbon generation peak, one is at 420℃~450℃(VR0 is 1.1%), another is at 450℃~500℃(VR0 is 2.0%);
     丝质体有两个生烃高峰 ,所对应的 VR0 (% )分别为 1.1%和 2 .0 % ;
短句来源
     After primary hydrocarbon generation, if the vitrinite reflectance is about 0.7%-0.9%, the re_generation peak will come in advance. When the reflectance is between 0.9% and 1.3%, the re_generation peak will be delayed.
     若反射率为0.9%~1.3%时,二次生烃高峰滞后;
短句来源
     When the reflectance is higher than 1.3%, the re_generation peak will be the same as that of the initial generation.
     而反射率>1.3%以后,二次生烃高峰与初次生烃连续.
短句来源
     It was considered that high palaeogeothermal system in Junggar basin caused early mature and hydrocarbon generation of Lower Permian source rocks and most of them were at hydrocarbon generation peak in the end of the Triassic, and almost at the same time, the deep traps of central Junggar basin basically falled into a pattern in the end of the Triassic or some early time before the Triassic, and in addition they were extremely matched with hydrocarbon generation history, which could result in hydrocarbon accumulation before the end of Triassic.
     准噶尔盆地古地温较高 ,使下二叠统烃源岩在三叠纪末大部分达到生烃高峰 ,而盆地腹部的深层圈闭在三叠纪末期或更早就已基本定型 ,与生烃史有很好的配置关系 ,因此深层油气在三叠纪末期以前就可聚集成藏 ;
短句来源
     The balanceable surface superimposition of Upper Paleozoic basin makes R_O of Lower Paleozoic higher than Upper Paleozoic,and the difference is more than 0.3%. So in the end of Triassic,Lower Paleozoic source rock achieved hydrocarbon generation peak,which expensed the initial organic matter and reduced the potentials of secondary hydrocarbon generation to some extent.
     上古生界盆地的均衡面式叠合使下古生界的热演化程度比上古生界至少高0.3%以上,因此,在三叠纪末下古生界基本达到生烃高峰,在一定程度上损耗了其原始有机质并降低其“二次生烃”潜力。
短句来源
  “generation peak”译为未确定词的双语例句
     The main source rock of Daqing oil field hydrocarbon accumulation system got into oil window at 77. 4 Ma, the generation peak period was between 73Ma to 65Ma.
     大庆油田成藏动力学系统内主要烃源岩在77.4Ma进入生油门限,73~65Ma为生油高峰期。
短句来源
     The Carboniferous and Permian source beds in a few major depressions of the basin reached the oil generation peak stage during Permian and Triassic Periods,therefore, the authors suggest that emphasis should be placed on finding Cenozoic reservoirs coupled with Paleozoic source beds.
     盆地中几个主要凹陷内石炭、二叠系生油岩在二叠、三叠纪时就进入了生油高峰期,因之应特别重视寻找古生新储的油气藏。
短句来源
     The results of FS indicate that, the larger of the area ratio between the fluorescence peak ( F ) and the second harmonic generation peak ( R ), the larger the first order constants of the photocatalytic reactions of SSal.
     Ti O2 荧光光谱的荧光峰面积(F )和倍频峰面积 (R)的比值越大 ,Ti O2 光催化降解 SSal的活性越高 . 提出了氢还原后 Ti O2 的光催化作用机制
短句来源
     No matter how the initial maturity, there is a hydrocarbon generation peak in the process of the hydrocarbon regeneration of the sedimentary organic matters, and it is lager than that of the continuous hydrocarbon generation. The lagging is enhanced with the initial maturity increasing.
     沉积有机质二次生烃量与初始成熟度和二次生烃终止成熟度密切相关,起始成熟度处于成熟早期—中期(Ro0.5%~0.9%),二次累积生烃量大于一次连续生烃量,且随起始成熟度增高,二者差值越来越大;
短句来源
     For type Ⅰ or Ⅱ kerogen ,most of natural gas is derived from cracking of oil generated from source rock during oil generation peak, only part of natural gas is originated from kerogen cracking directly. Genetic identification of kerogen and oil cracked gases is very important for the study of natural gas sources and area exploration evaluation , especially for high maturity areas.
     对于腐泥型有机质 ,绝大部分天然气是来自源岩生成的原油裂解气 ,只有部分来自干酪根的裂解气 ,因此天然气气源研究不仅要指出来自哪套源岩 ,还需指出它的成因 ,尤其是高演化地区天然气气源研究。
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  generation peak
New Zealand currently has approximately 168 MW of installed wind capacity, and a system generation peak of approximately 6600 MW.
      


The authors studied 41 samples of kerogen from the Eogene HetaoyuanFormation in Biyang Depression,Henan by ETIR technique.Oxygen-bearingfunctional group decreases with the increase of buried depth,and completelydisappeared at 3500m.Alkyl group increases to a peak value with theincrease of buried depth,and then decreases gradually.The depth of peak-value shows identity with that of oil-generating peak.Aromatic rings showa little change near the threshold depth of oil-generation but increases obvi-ously below...

The authors studied 41 samples of kerogen from the Eogene HetaoyuanFormation in Biyang Depression,Henan by ETIR technique.Oxygen-bearingfunctional group decreases with the increase of buried depth,and completelydisappeared at 3500m.Alkyl group increases to a peak value with theincrease of buried depth,and then decreases gradually.The depth of peak-value shows identity with that of oil-generating peak.Aromatic rings showa little change near the threshold depth of oil-generation but increases obvi-ously below the depth of oil-generation peak.

作者用红外光谱仪分析了泌阳凹陷生油岩干酪根,研究了干酪根中烷基、含氧官能团和芳环的变化规律。含氧官能团随埋深逐渐减少,到达一定深度后完全消失;烷基具有明显的高峰区,这个高峰与生油高峰是一致的;芳环在生油门限前后比较稳定,生油高峰过后明显增加。

The major source beds in the oil— bearing basins of Xinjiang are Paleozoic formations, therefore, it is rather important to study the paleogeothermal regimes of the basins.For the further study of the geothermal histories of the basins, the method of fission scar tracks in apatite is adopted, which suggests that the annealing temperatures (70~125℃) of fission tracks in apatite are within the temperature range (60~110℃) of substantial oil generation. Besides, the method is also used for solving the thermal history...

The major source beds in the oil— bearing basins of Xinjiang are Paleozoic formations, therefore, it is rather important to study the paleogeothermal regimes of the basins.For the further study of the geothermal histories of the basins, the method of fission scar tracks in apatite is adopted, which suggests that the annealing temperatures (70~125℃) of fission tracks in apatite are within the temperature range (60~110℃) of substantial oil generation. Besides, the method is also used for solving the thermal history and some basic geological problems of sedimentary basins. The age of fission tracks represents the geological age of uplifting and erosion, s(?) it can be used for the timing of uplifting and erosion. The authors suppose a method of reconstructing geothermal history using enclosure temperature.The geothermal evolution of the Junggar Basin is divided into three major phases: a) the geosynclinal phase (Carboniferous Period) with paleothermal gradients, of 8~5 C/100m, b) the foredeep phase (Permian to the end of Triassic Period) with paleothermal gradients of 5~3℃ 100 m, and c) the platform phase (Jurassic to Paleogene) with paleothermal gradient of 3~2℃ 100 m. The Carboniferous and Permian source beds in a few major depressions of the basin reached the oil generation peak stage during Permian and Triassic Periods,therefore, the authors suggest that emphasis should be placed on finding Cenozoic reservoirs coupled with Paleozoic source beds.

新疆含油气盆地的主要生油层是古生界,研究盆地的古地温显得尤为重要。 为进一步研究盆地的热史,引进了裂变径迹法,即磷灰石裂变径迹退火带上—下限温度为70~125℃。同石油主要形成于60~140℃之间相接近。此方法还可解决沉积盆地热历史及某些基础地质问题。裂变径迹年龄代表抬升剥蚀以后的地质年龄,可推断抬升剥蚀作用发生的时间。提出了用包裹体溫度认识地热过程。 准噶尔盆地地溫演化可分为三个主要阶段:地槽期(石炭纪时期)古地温梯度8~5℃/100m:山前坳陷期(二叠—三叠纪末)古地温梯度5~3℃/100m:地台期(侏罗—早第三纪)古地温梯度3~2℃/100m。盆地中几个主要凹陷内石炭、二叠系生油岩在二叠、三叠纪时就进入了生油高峰期,因之应特别重视寻找古生新储的油气藏。

The author of this paper describes four principal factors for the formation of nautral gas pools under a dynamic balance regime based on the relationship between the generation, accumulation and dissipation of natural gas.The source rocks and the stage of gas generation peak are the most important factors in the formation of gas pool while sealing efficiency and tectonic settings are the important factors for the gas accumulation and dissipation. Therefore, it is concluded that four fundamental factros...

The author of this paper describes four principal factors for the formation of nautral gas pools under a dynamic balance regime based on the relationship between the generation, accumulation and dissipation of natural gas.The source rocks and the stage of gas generation peak are the most important factors in the formation of gas pool while sealing efficiency and tectonic settings are the important factors for the gas accumulation and dissipation. Therefore, it is concluded that four fundamental factros for the formation of natural gas pools are of abundant gas source, the late stage of gas generation peak, excellent sealing efficiency and stable teete-nic settings.

作者根据天然气的生成、聚集与散失之间的动态平衡关系,对天然气动态平衡成藏的四个基本条件进行论述。在生成方面,主要是气源和生气高峰:在聚集与散失方面,主要是封盖条件和构造环境。归纳行来即:充沛的气源、生气高峰的时代越新越好、良好的封盖条件和比较稳定的后期构造环境。

 
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